“…They exhibit classical shalelimestone alternations of the Early Triassic Thaynes Group (sensu Lucas et al, 2007), which represent relatively shallow sedimentary deposits in an epicontinental sea. The maximum extent of this epicontinental sea within the western USA basin occurred during the Smithian-Spathian transition (Lucas et al, 2007;Brayard et al, 2013Brayard et al, , 2020Vennin et al, 2015;Olivier et al, 2018) and was probably controlled by a North-South differentiation in regional tectonics (Caravaca et al, 2018) and by concurrent global climatic changes (e.g., .…”